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Constraining the ocean’s biological pump with in situ optical observations and supervised learning. Part 1:particle size distributions
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  • Daniel J Clements,
  • Simon Yang,
  • Thomas Weber,
  • Andrew McDonnell,
  • Rainer Kiko,
  • Lars Stemmann,
  • Daniele Bianchi
Daniel J Clements
Department of Atmospheric and Oceanic Sciences, University of California Los Angeles, Los Angeles, CA, USA.

Corresponding Author:[email protected]

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Simon Yang
Department of Atmospheric and Oceanic Sciences, University of California Los Angeles, Los Angeles, CA, USA.
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Thomas Weber
Department of Earth and Environmental Sciences, University of Rochester,Rochester, New York, USA
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Andrew McDonnell
College of Fisheries and Ocean Sciences, University of Alaska Fairbanks, Fairbanks, Alaska 99775-7220, USA.
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Rainer Kiko
Sorbonne Université
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Lars Stemmann
Sorbonne Université, CNRS, UMR 7093, Institut de la Mer de Villefranche sur mer, Laboratoire d’Océanographie de Villefranche, Villefranche-sur-Mer, France.
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Daniele Bianchi
Department of Atmospheric and Oceanic Sciences, University of California Los Angeles, Los Angeles, CA, USA.
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Abstract

The abundance and size distribution of marine organic particles are two major factors controlling biological carbon sequestration in the ocean. These quantities are the result of complex physical-biological interactions that are difficult to observe, and their spatial and temporal patterns remain uncertain. Here, we present a novel analysis of particle size distributions (PSD) from a global compilation of in situ Underwater Vision Profiler 5 (UVP5) optical measurements. Using a machine learning algorithm, we extrapolate sparse UVP5 observations to the global ocean from well-sampled oceanographic variables. We reconstruct global maps of PSD parameters (biovolume and slope) for particles at the base of the euphotic zone. These reconstructions reveal consistent global patterns, with high chlorophyll regions generally characterized by high particle biovolume and flatter PSD slope, i.e., a high relative abundance of large vs. small particles. The resulting negative correlations between particle biovolume and slope further suggests amplified effects on sinking particle fluxes. Our approach and estimates provide a baseline for an improved understanding of particle cycles in the ocean, and pave the way to global, three-dimensional reconstructions of sinking particle fluxes from UVP5 observations.